Author/Authors :
M. Hornung، نويسنده , , K. R. Bull، نويسنده , , M. Cresser، نويسنده , , J. Hall، نويسنده , , S. J. Langan، نويسنده , , Jonathan P. Loveland، نويسنده , , C. Smith، نويسنده ,
Abstract :
The method used to produce a critical load map of acidity for soils in Great Britain is described. Critical loads were assigned to the dominant soil in each 1 km grid square of the UK national grid. Mineral soils were assigned a critical load based on mineralogy and chemistry, using approaches appropriate to UK conditions. Critical loads for peat soils are based primarily on a maximum acceptable reduction of peat pH, and results from laboratory equilibration studies. The map shows that soils with small critical loads (<0.5 kmolc ha−1 year−1) i.e. highly sensitive to acidic deposition, dominate in the north and west of Britain; the south and east are dominated by soils with large critical loads, with small areas of more sensitive soils associated with sandy soil-forming materials. A modified critical load map illustrates the potential impact of agricultural liming on soil critical loads.